The Giza Pyramid Complex also called the Giza Necropolis, is the site on the Giza Plateau in Greater Cairo, Egypt that includes the Great Pyramid of Giza, the Pyramid of Khafre, and the Pyramid of Menkaure, along with their associated pyramid complexes and the Great Sphinx of Giza. All were built during the Fourth Dynasty of the Old Kingdom of Ancient Egypt. The site also includes several cemeteries and the remains of a worker’s village.

The site is at the edges of the Western Desert, approximately 9 kilometers west of the Nile River in the city of Giza, and about 13 kilometers southwest of the city center of Cairo.

The Great Pyramid and the Pyramid of Khafre are the largest pyramids built in ancient Egypt, and they have historically been common as emblems of Ancient Egypt in the Western imagination. They were popularized in Hellenistic times when the Great Pyramid was listed by Antipater of Sidon as one of the Seven Wonders of the World. It is by far the oldest of the Ancient Wonders and the only one still in existence.
Pyramids and Sphinx

Giza pyramid complex

Pyramids of Gizeh. 1893. Egypt; heliogravure after original views. Wilbour Library of Egyptology. Brooklyn Museum
The Giza pyramid complex consists of the Great Pyramid (also known as the Pyramid of Cheops or Khufu and constructed, the somewhat smaller Pyramid of Khafre (or Chephren) a few hundred meters to the south-west, and the relatively modest-sized Pyramid of Menkaure (or Mykerinos) a few hundred meters farther south-west. The Great Sphinx lies on the east side of the complex. The current consensus among Egyptologists is that the head of the Great Sphinx is that of Khafre. Along with these major monuments are a number of smaller satellite edifices, known as “queens” pyramids, causeways, and valley pyramids

Khufu’s complex
Main article: Great Pyramid of Giza
Khufu’s pyramid complex consists of a valley temple, now buried beneath the village of Nazlet el-Samman; diabase paving and nummulitic limestone walls have been found but the site has not been excavated, The valley temple was connected to a causeway which was largely destroyed when the village was constructed. The causeway led to the Mortuary Temple of Khufu. Of this temple, the basalt pavement is the only thing that remains. The mortuary temple was connected to the king’s pyramid. The king’s pyramid, completed in 2560 BC, has three smaller queen’s pyramids associated with it and three boat pits. The boat pits contained a ship, and the two pits on the south side of the pyramid still contained intact ships when excavated. One of these ships, the Khufu ship, has been restored and is on display at the Giza Solar boat museum.

Khufu’s pyramid still has a limited number of casing stones at its base. These casing stones were made of fine white limestone quarried from the nearby range.

Khafre’s complex
Main articles: Pyramid of Khafre and Great Sphinx of Giza
Khafre’s pyramid complex consists of a valley temple, the Sphinx temple, a causeway, a mortuary temple, and the king’s pyramid. The valley temple yielded several statues of Khafre. Several were found in a well on the floor of the temple by Mariette in 1860. Others were found during successive excavations by Sieglin (1909–10), Junker, Reisner, and Hassan. Khafre’s complex contained five boat-pits and a subsidiary pyramid with a serdab.:19–26 Khafre’s pyramid, completed in 2570 BC, appears larger than the adjacent Khufu Pyramid by virtue of its more elevated location, and the steeper angle of inclination of its construction—it is, in fact, smaller in both height and volume. Khafre’s pyramid retains a prominent display of casing stones at its apex.

Menkaure’s complex
Main article: Pyramid of Menkaure
Menkaure’s pyramid complex consists of a valley temple, a causeway, a mortuary temple, and the king’s pyramid. The valley temple once contained several statues of Menkaure. During the 5th Dynasty, a smaller ante-temple was added to the valley temple. The mortuary temple also yielded several statues of Menkaure. The king’s pyramid, completed ca. 2510 BC, has three subsidiaries or queen’s pyramids.:26–35 Of the four major monuments, only Menkaure’s pyramid is seen today without any of its original polished limestone casing.

Sphinx
Main article: Great Sphinx of Giza
The Sphinx dates from the reign of king Khafre. During the New Kingdom, Amenhotep II dedicated a new temple to Hauron-Haremakhet, and this structure was added onto by later rulers

Construction
Main article: Egyptian pyramid construction techniques
Most construction theories are based on the idea that the pyramids were built by moving huge stones from a quarry and dragging and lifting them into place. The disagreements center on the method by which the stones were conveyed and placed and how possible the method was.

In building the pyramids, the architects might have developed their techniques over time. They would select a site on a relatively flat area of bedrock—not sand—which provided a stable foundation. After carefully surveying the site and laying down the first level of stones, they constructed the pyramids in horizontal levels, one on top of the other.

For the Great Pyramid, most of the stone for the interior seems to have been quarried immediately to the south of the construction site. The smooth exterior of the pyramid was made of a fine grade of white limestone that was quarried across the Nile. These exterior blocks had to be carefully cut, transported by river barge to Giza, and dragged up ramps to the construction site. Only a few exterior blocks remain in place at the bottom of the Great Pyramid. During the Middle Ages (5th century to 15th century), people may have taken the rest away for building projects in the city of Cairo.

To ensure that the pyramid remained symmetrical, the exterior casing stones all had to be equal in height and width. Workers might have marked all the blocks to indicate the angle of the pyramid wall and trimmed the surfaces carefully so that the blocks fit together. During construction, the outer surface of the stone was smooth limestone; excess stone has eroded as time has passed

Purpose
The pyramids of Giza and others are thought to have been constructed to house the remains of the deceased Pharaohs who ruled over Ancient Egypt. A portion of the pharaoh’s spirit called his ka was believed to remain with his corpse. Proper care of the remains was necessary in order for the “former Pharaoh to perform his new duties as king of the dead”. It is theorized the pyramid not only served as a tomb for the pharaoh but also as a storage pit for various items he would need in the afterlife. “The people of Ancient Egypt believed that death on Earth was the start of a journey to the next world.” The embalmed body of the King was entombed underneath or within the pyramid to protect it and allow his transformation and ascension to the afterlife.

Astronomy

The Giza pyramid complex at night
The sides of all three of the Giza pyramids were astronomically oriented to the north-south and east-west within a small fraction of a degree. Among recent attempts to explain such a clearly deliberate pattern are those of S. Haack, O. Neugebauer, K. Spence, D. Rawlins, K. Pickering, and J. Belmonte. The arrangement of the pyramids is a representation of the Orion constellation according to the disputed Orion correlation theory.

there are special organized tours to the area

The Valley of the Kings, also known as the Valley of the Gates of the Kings is a valley in Egypt where, for a period of nearly 500 years from the 16th to 11th century BC, rock-cut tombs were excavated for the pharaohs and powerful nobles of the New Kingdom (the Eighteenth to the Twentieth Dynasties of Ancient Egypt).

The valley stands on the west bank of the Nile, opposite Thebes (modern Luxor), within the heart of the Theban Necropolis The wadi consists of two valleys, East Valley (where the majority of the royal tombs are situated) and West Valley.

With the 2005 discovery of a new chamber and the 2008 discovery of two further tomb entrances, the valley is known to contain 64 tombs and chambers (ranging in size from KV54, a simple pit, to KV5, a complex tomb with over 120 chambers). It was the principal burial place of the major royal figures of the Egyptian New Kingdom, as well as a number of privileged nobles. The royal tombs are decorated with scenes from Egyptian mythology and give clues as to the beliefs and funerary practices of the period. Almost all of the tombs seem to have been opened and robbed in antiquity, but they still give an idea of the opulence and power of the pharaohs.

This area has been a focus of archaeological and Egyptological exploration since the end of the eighteenth century, and its tombs and burials continue to stimulate research and interest. In modern times the valley has become famous for the discovery of the tomb of Tutankhamun (with its rumors of the curse of the pharaohs) and is one of the most famous archaeological sites in the world. In 1979, it became a World Heritage Site, along with the rest of the Theban Necropolis.[9] Exploration, excavation, and conservation continue in the valley, and a new tourist center has recently been opened.

Royal Necropolis
The official name for the site in ancient times was The Great and Majestic Necropolis of the Millions of Years of the Pharaoh, Life, Strength, Health in The West of Thebes (see below for the hieroglyphic spelling), or Ta-sekhet-ma’at (the Great Field).

In the Eighteenth Dynasty, only kings were buried within the valley in large tombs. When a non-royal person was buried, it was in a small rock-cut chamber, close to the tomb of their master, Amenhotep III’s tomb was constructed in the Western Valley, and while his son Akhenaten moved his tomb’s construction to Amarna, it is thought that the unfinished WV25 may have originally been intended for him. With the return to religious orthodoxy at the end of the Eighteenth Dynasty, Tutankhamun, Ay, and Horemheb returned to the royal necropolis.

The Nineteenth and Twentieth Dynasties saw an increase in the number of burials (both here and in the Valley of the Queens), with Ramesses II and later Ramesses III each constructing a massive tomb used for the burial of their sons (KV5 and KV3 respectively). There are some kings that are not buried within the valley or whose tomb has not been located: Thutmose II may have been buried in Dra’ Abu el-Naga’ (although his mummy was in the Deir el-Bahari tomb cache), Smenkhkare’s burial has never been located, and Ramesses VIII seems to have been buried elsewhere.

In the Pyramid Age, the pyramid tomb of a king was associated with a mortuary temple located close to the pyramid. Since the tombs of the kings in the Valley of the Kings were hidden, the kings’ mortuary temples were located away from their burial sites, closer to the cultivation facing Thebes. These mortuary temples became places visited during the various festivals held in the Theban necropolis. Most notable is the Beautiful festival of the valley, where the sacred barques of Amun-Re, his consort, Mut, and son, Khonsu, left the temple at Karnak in order to visit the funerary temples of deceased kings on the West Bank and their shrines in the Theban Necropolis

The tombs were constructed and decorated by the workers of the village of Deir el-Medina, located in a small wadi between this valley and the Valley of the Queens, facing Thebes. The workers journeyed to the tombs through various routes over the Theban hills. The daily lives of these workers are quite well known due to their being recorded in tombs and official documents.[39] Amongst the events documented is perhaps the first recorded workers’ strike, detailed in the Turin Strike Papyrus.

Exploration of the valley
Main article: Exploration of the Valley of the Kings
View of the central East Valley, showing area around KV62
The valley has been a major focus of modern Egyptological exploration for the last two centuries. Prior to this time, it was a site for tourism in antiquity (especially during Roman times).[29] The area illustrates the changes in the study of ancient Egypt, starting as antiquity hunting, and ending as the scientific excavation of the whole Theban Necropolis. Despite the exploration and investigation noted below, only eleven of the tombs have actually been completely recorded.

Many of the tombs have graffiti written by those ancient tourists. Jules Baillet has located over 2,100 Greek and Latin instances of graffiti, along with a smaller number in Phoenician, Cypriot, Lycian, Coptic, and other languages.[29] The majority of the ancient graffiti is found in KV9, which contains just under a thousand of them. The earliest positively dated graffiti dates to 278 B.C.

Entrance to a royal tomb, drawn in 1821
In 1799, members of Napoleon’s expedition to Egypt (especially Vivant Denon) drew maps and plans of the known tombs, and for the first time noted the Western Valley (where Prosper Jollois and Édouard de Villiers du Terrage located the tomb of Amenhotep III, WV22). The Description de l’Égypte contains two volumes (out of a total of 24) on the area around Thebes.

European exploration continued in the area around Thebes during the nineteenth century. Early in the century, the area was visited by Giovanni Belzoni, working for Henry Salt, who discovered several tombs, including those of Ay in the West Valley (WV23) in 1816 and Seti I (KV17) the following year. At the end of his visits, Belzoni declared that all of the tombs had been located and nothing of note remained to be found. Working at the same time was Bernardino Drovetti, the French Consul-General and a great rival of Belzoni and Salt.[46] John Gardner Wilkinson, who lived in Egypt from 1821 to 1832, copied many of the inscriptions and artwork in the tombs that were open at the time. The decipherment of hieroglyphs, though still incomplete during Wilkinson’s stay in the valley, enabled him to assemble a chronology of New Kingdom rulers based on the inscriptions in the tombs. He also established the system of tomb numbering that has been in use, with additions, ever since

The second half of the century saw a more concerted effort to preserve, rather than simply gather, antiquities. Auguste Mariette’s Egyptian Antiquities Service started to explore the valley, first with Eugène Lefébure in 1883,[48] then Jules Baillet and Georges Bénédite in early 1888, and finally Victor Loret in 1898 to 1899. Loret added a further 16 tombs to the list, and explored several tombs that had already been discovered During this time Georges Daressy explored KV9.

When Gaston Maspero was reappointed as head of the Egyptian Antiquities Service, the nature of the exploration of the valley changed again. Maspero appointed English archaeologist Howard Carter as the Chief Inspector of Upper Egypt, and the young man discovered several new tombs and explored several others, clearing KV42 and KV20.

Entrance to Horemheb’s tomb, soon after its discovery in 1908
Around the start of the 20th century, American explorer Theodore M. Davis had the excavation permit for the valley. His team (led mostly by Edward R. Ayrton) discovered several royal and non-royal tombs (including KV43, KV46 and KV57). In 1907, they discovered the possible Amarna Period cache in KV55. After finding what they thought was all that remained of the burial of Tutankhamun (items recovered from KV54 and KV58), it was announced that the valley was completely explored and that no further burials were to be found. Davis’s 1912 publication, The Tombs of Harmhabi and Touatânkhamanou closes with the comment, “I fear that the Valley of Kings is now exhausted.”

After Davis’s death early in 1915, Lord Carnarvon acquired the concession to excavate the valley, and he employed Howard Carter to explore it. After a systematic search, they discovered the actual tomb of Tutankhamun (KV62) in November 1922.

Various expeditions have continued to explore the valley, adding greatly to the knowledge of the area. In 2001 the Theban Mapping Project designed new signs for the tombs, providing information and plans of the open tombs

there are special organized tours to the area

Sinai Peninsula, Arabic Shibh Jazīrat Sīnāʾ, triangular peninsula linking Africa with Asia and occupying an area of 23,500 square miles (61,000 square km). The Sinai Desert, as the peninsula’s arid expanse is called, is separated by the Gulf of Suez and the Suez Canal from the Eastern Desert of Egypt, but it continues eastward into the Negev desert without marked change of relief. Usually regarded as being geographically part of Asia, the Sinai Peninsula is the northeastern extremity of Egypt and adjoins Israel and the Gaza Strip on the east. The Sinai is administratively divided into two muḥāfaẓahs (governorates): Shamāl Sīnāʾ in the north and Janūb Sīnāʾ in the south. The peninsula was occupied by Israeli forces during the Six-Day War of June 1967 but was returned to Egypt in 1982 under the terms of the peace treaty concluded between those countries in 1979

Geography
The Sinai Peninsula lies between the Gulf of Suez and the Suez Canal on the west and the Gulf of Aqaba and the Negev on the east, and it is bounded by the Mediterranean Sea on the north and the Red Sea to the south. Its greatest dimensions are about 130 miles (210 km) from east to west and about 240 miles (385 km) from north to south.

History
The Sinai has been inhabited since prehistoric times. The earliest written information about it dates from 3000 BCE, when the ancient Egyptians recorded their explorations there in search of copper ores. The passage of the Israelites through the Sinai is undoubted, but the route and the date of their Exodus are still matters of debate. The Sinai is likewise famous as the scene of the giving of the Law to Moses, but there is doubt as to which of the mountains there is the actual site. A road along the Sinai’s northern coast served as the principal trade route between Egypt and Palestine for many centuries, and it is likely that Egypt erected a chain of fortresses to guard this route. After the decline of the Egyptian empire, Nabataeans from Petra controlled the trade routes of the Sinai for two centuries, until they were defeated by the Romans in 106 CE. The region then became part of the province of Arabia in the Roman Empire.

During the early Christian period, the Sinai became the home of a large number of hermits and ascetics, particularly in the mountainous southern region. In 530 CE the Byzantine emperor Justinian I began building the monastery of St. Catherine on the lower slopes of Mount Sinai. This provided a center for the scattered communities of Christians in the area, and the monastery served as a pilgrimage site throughout the Middle Ages. After 1517 the Sinai formed part of the Ottoman Empire and was administered by an official sent from Constantinople (now Istanbul). Conditions in the Sinai deteriorated, and traveling there became difficult after Egypt became independent of direct Turkish rule in the early 19th century. The Al-ʿArīsh area was the scene of fighting between the Turks and the British during World War I, and at the war’s end, the Sinai was turned over to Egypt.

The Sinai was administered by Egypt until the Israelis overran the peninsula in the Six-Day War of June 1967. It was the focus of Israeli-Egyptian combat in every military confrontation between the two countries from 1949 to 1973, the Giddy and Mitla pass in the peninsula’s northeastern portion being the scene of bitter fighting in 1956, 1967, and 1973. (See Arab-Israeli wars.) Following the peace agreement reached between Egypt and Israel in 1979, the Sinai Peninsula was returned to Egypt and demilitarized under the terms of the agreement. The peninsula was later the site of a number of attacks by militant Islamist groups; primarily targeting tourists, the attacks included those in Ṭābā (and elsewhere) in October 2004, in Sharm el-Sheikh in July 2005, and in Dhahab in April 2006. Egyptian military personnel and civilian residents of the peninsula became the focus of attacks in the 2010s after the Egyptian Uprising of 2011 exacerbated a security vacuum. On November 24, 2017, an attack on a Sufi mosque in Al-Rawḍah (near Al-ʿArīsh) killed some 300 worshippers in the deadliest terrorist attack in Egyptian history.

Demographics

Two young Bedouins making bread in the desert
The two governorates of North and South Sinai have a total population of 597,000 (January 2013). This figure rises to 1,400,000 by including Western Sinai, the parts of the Port Said, Ismailia, and Suez Governorates lying east of the Suez Canal. Port Said alone has a population of roughly 500,000 people (January 2013). Portions of the populations of Ismailia and Suez live in west Sinai, while the rest live on the western side of the Suez Canal.

The population of Sinai has largely consisted of desert-dwelling Bedouins with their colorful traditional costumes and significant culture.[31] Large numbers of Egyptians from the Nile Valley and Delta moved to the area to work in tourism, but development adversely affected the native Bedouin population.[citation needed] In order to help alleviate their problems, various NGOs began to operate in the region, including the Makhad Trust, a UK charity that assists the Bedouin in developing a sustainable income while protecting Sinai’s natural environment, heritage, and culture

Economy
Since the Israeli–Egyptian peace treaty, Sinai‘s scenic spots (including coral reefs offshore) and religious structures have become important to the tourism industry. The most popular tourist destination in Sinai are Mount Sinai (Jabal Musa) and St Catherine’s Monastery, which is considered to be the oldest working Christian monastery in the world, and the beach resorts of Sharm el-Sheikh, Dahab, Nuweiba, and Taba. Most tourists arrive at Sharm el-Sheikh International Airport, through Eilat, Israel, and the Taba Border Crossing, by road from Cairo or by ferry from Aqaba in Jordan

there are special organized tours to the area

Egypt officially the Arab Republic of Egypt is a transcontinental country spanning the northeast corner of Africa and southwest corner of Asia by a land bridge formed by the Sinai Peninsula. Egypt is a Mediterranean country bordered by the Gaza Strip (Palestine) and Israel to the northeast, the Gulf of Aqaba and the Red Sea to the east, Sudan to the south, and Libya to the west. Across the Gulf of Aqaba lies Jordan, across the Red Sea lies Saudi Arabia, and across the Mediterranean lies Greece, Turkey, and Cyprus, although none share a land border with Egypt.

Egypt has one of the longest histories of any country, tracing its heritage along the Nile Delta back to the 6th–4th millennia BCE. Considered a cradle of civilization, Ancient Egypt saw some of the earliest developments of writing, agriculture, urbanization, organized religion, and central government.[12] Iconic monuments such as the Giza Necropolis and its Great Sphinx, as well the ruins of Memphis, Thebes, Karnak, and the Valley of the Kings, reflect this legacy and remain a significant focus of scientific and popular interest. Egypt’s long and rich cultural heritage is an integral part of its national identity, which has endured and often assimilated, various foreign influences, including Greek, Persian, Roman, Arab, Ottoman Turkish, and Nubian. Egypt was an early and important center of Christianity, but was largely Islamised in the seventh century and remains a predominantly Muslim country, albeit with a significant Christian minority.

Modern Egypt dates back to 1922 when it gained independence from the British Empire as a monarchy. Following the 1952 revolution, Egypt declared itself a republic, and in 1958 it merged with Syria to form the United Arab Republic, which dissolved in 1961. Throughout the second half of the 20th century, Egypt endured social and religious strife and political instability, fighting several armed conflicts with Israel in 1948, 1956, 1967, and 1973, and occupying the Gaza Strip intermittently until 1967. In 1978, Egypt signed the Camp David Accords, officially withdrawing from the Gaza Strip and recognizing Israel. The country continues to face challenges, from political unrest, including the recent 2011 revolution and its aftermath, to terrorism and economic underdevelopment. Egypt’s current government, a semi-presidential republic has been described by a number of watchdogs as authoritarian or heading an authoritarian regime, responsible for perpetuating the country’s problematic human rights record.

Islam is the official religion of Egypt and Arabic is its official language. With over 100 million inhabitants, Egypt is the most populous country in North Africa, the Middle East, and the Arab world, the third-most populous in Africa (after Nigeria and Ethiopia), and the thirteenth most populous in the world. The great majority of its people live near the banks of the Nile River, an area of about 40,000 square kilometers (15,000 sq mi), where the only arable land is found. The large regions of the Sahara desert, which constitute most of Egypt’s territory, are sparsely inhabited. About half of Egypt’s residents live in urban areas, with most spread across the densely populated centers of greater Cairo, Alexandria, and other major cities in the Nile Delta.

Geography
Egypt is considered to be a regional power in North Africa, the Middle East, and the Muslim world, and a middle power worldwide.[14] With one of the largest and most diversified economies in the Middle East, which is projected to become one of the largest in the world in the 21st century, Egypt has the third-largest economy in Africa, the world’s 40th-largest economy by nominal GDP, and the 19-largest by PPP. Egypt is a founding member of the United Nations, the Non-Aligned Movement, the Arab League, the African Union, and the Organisation of Islamic Cooperation.
Egypt lies primarily between latitudes 22° and 32°N, and longitudes 25° and 35°E. At 1,001,450 square kilometres (386,660 sq mi),[112] it is the world’s 30th-largest country. Due to the extreme aridity of Egypt’s climate, population centers are concentrated along the narrow Nile Valley and Delta, meaning that about 99% of the population uses about 5.5% of the total land area. 98% of Egyptians live on 3% of the territory.

Egypt is bordered by Libya to the west, Sudan to the south, and the Gaza Strip and Israel to the east. Egypt’s important role in geopolitics stems from its strategic position: a transcontinental nation, it possesses a land bridge (the Isthmus of Suez) between Africa and Asia, traversed by a navigable waterway (the Suez Canal) that connects the Mediterranean Sea with the Indian Ocean by way of the Red Sea.

Apart from the Nile Valley, the majority of Egypt’s landscape is desert, with a few oases scattered about. Winds create prolific sand dunes that peak at more than 30 meters (100 ft) high. Egypt includes parts of the Sahara desert and of the Libyan Desert. These deserts protected the Kingdom of the Pharaohs from western threats and were referred to as the “red land” in ancient Egypt.

Towns and cities include Alexandria, the second-largest city; Aswan; Asyut; Cairo, the modern Egyptian capital and largest city; El Mahalla El Kubra; Giza, the site of the Pyramid of Khufu; Hurghada; Luxor; Kom Ombo; Port Safaga; Port Said; Sharm El Sheikh; Suez, where the south end of the Suez Canal is located; Zagazig; and Minya. Oases include Bahariya, Dakhla, Farafra, Kharga, and Siwa. Protectorates include Ras Mohamed National Park, Zaranik Protectorate, and Siwa.

On 13 March 2015, plans for a proposed new capital of Egypt were announced
Economy
Egypt’s economy depends mainly on agriculture, media, petroleum imports, natural gas, and tourism; there are also more than three million Egyptians working abroad, mainly in Libya, Saudi Arabia, the Persian Gulf, and Europe. The completion of the Aswan High Dam in 1970 and the resultant Lake Nasser have altered the time-honored place of the Nile River in the agriculture and ecology of Egypt. A rapidly growing population, limited arable land, and dependence on the Nile all continue to overtax resources and stress the economy.

Egypt has a developed energy market based on coal, oil, natural gas, and hydropower. Substantial coal deposits in the northeast Sinai are mined at the rate of about 600,000 tonnes (590,000 long tons; 660,000 short tons) per year. Oil and gas are produced in the western desert regions, the Gulf of Suez, and the Nile Delta. Egypt has huge reserves of gas, estimated at 2,180 cubic kilometers (520 cu mi),[201] and LNG up to 2012 exported to many countries. In 2013, the Egyptian General Petroleum Co (EGPC) said the country will cut exports of natural gas and tell major industries to slow output this summer to avoid an energy crisis and stave off political unrest, Reuters has reported. Egypt is counting on top liquid natural gas (LNG) exporter Qatar to obtain additional gas volumes in summer while encouraging factories to plan their annual maintenance for those months of peak demand, said EGPC chairman, Tarek El Barkatawy. Egypt produces its own energy, but has been a net oil importer since 2008 and is rapidly becoming a net importer of natural gas
Economic conditions have started to improve considerably, after a period of stagnation, due to the adoption of more liberal economic policies by the government as well as increased revenues from tourism and a booming stock market. In its annual report, the International Monetary Fund (IMF) has rated Egypt as one of the top countries in the world undertaking economic reforms.[203] Some major economic reforms undertaken by the government since 2003 include a dramatic slashing of customs and tariffs. A new taxation law implemented in 2005 decreased corporate taxes from 40% to the current 20%, resulting in a stated 100% increase in tax revenue by the year 2006

Egyptian society is moderately unequal in terms of the income distribution, with an estimated 35–40% of Egypt’s population earning less than the equivalent of $2 a day, while only around 2–3% may be considered wealthy

there are several organized tours to discover the pharos land

Aswan is a city in the south of Egypt and is the capital of the Aswan Governorate.

Aswan is a busy market and tourist center located just north of the Aswan Dam on the east bank of the Nile at the first cataract. The modern city has expanded and includes the formerly separate community on the island of Elephantine.

The city is part of the UNESCO Creative Cities Network in the category of craft and folk art.[5]

Aswan is a large tourist city where a current population is 1,568,000.

Climate
Aswan has a hot desert climate like the rest of Egypt. Aswan and Luxor have the hottest summer days of any city in Egypt. Aswan is one of the hottest, sunniest and driest cities in the world. Average high temperatures are consistently above 40 °C (104.0 °F) during summer (June, July, August and also September) while average low temperatures remain above 25 °C (77.0 °F). Average high temperatures remain above 23 °C (73.4 °F) during the coldest month of the year while average low temperatures remain above 8 °C (46.4 °F). Summers are very prolonged and extremely hot with blazing sunshine although desert heat is dry. Winters are brief and pleasantly mild, though nights may be cool at times.

The climate of Aswan is extremely dry year-round, with less than 1 mm (0 in) of average annual precipitation. The desert city is one of the driest ones in the world, and rainfall doesn’t occur every year, as of early 2001, the last rain there was seven years earlier. Aswan is one of the least humid cities on the planet, with an average relative humidity of only 26%, with a maximum mean of 42% during winter and a minimum mean of 16% during summer.

The weather of Aswan is extremely clear, bright, and sunny year-round, in all seasons, with a low seasonal variation, with almost 4,000 hours of annual sunshine, very close to the maximum theoretical sunshine duration. Aswan is one of the sunniest places on Earth.

The highest record temperature was 51 °C (124 °F) on July 4, 1918, and the lowest record temperature was −2.4 °C (27.7 °F) on January 6, 1989.

History

Aswan is the ancient city of Swenett, later known as Syene, which in antiquity was the frontier town of Ancient Egypt facing the south. Swenett is supposed to have derived its name from an Egyptian goddess with the same name.[9] This goddess later was identified as Eileithyia by the Greeks and Lucina by the Romans during their occupation of Ancient Egypt because of the similar association of their goddesses with childbirth, and of which the import is “the opener”. The ancient name of the city also is said to be derived from the Egyptian symbol for “trade” or “market”
Because the Ancient Egyptians oriented themselves toward the origin of the life-giving waters of the Nile in the south, and as Swenett was the southernmost town in the country, Egypt always was conceived to “open” or begin at Swenett. The city stood upon a peninsula on the right (east) bank of the Nile, immediately below (and north of) the first cataract of the flowing waters, which extend to it from Philae. Navigation to the delta was possible from this location without encountering a barrier.

The stone quarries of ancient Egypt located here were celebrated for their stone, and especially for the granitic rock called Syenite. They furnished the colossal statues, obelisks, and monolithic shrines that are found throughout Egypt, including the pyramids; and the traces of the quarrymen who worked in these 3,000 years ago are still visible in the native rock. They lie on either bank of the Nile, and a road, 6.5 km (4.0 mi) in length, was cut beside them from Syene to Philae.

Swenett was equally important as a military station as a place of traffic. Under every dynasty, it was a garrison town, and here tolls and customs were levied on all boats passing southwards and northwards. Around 330, the legion stationed here received a bishop from Alexandria; this later became the Coptic Diocese of SyeneThe city is mentioned by numerous ancient writers, including Herodotus, Strabo, Stephanus of Byzantium, Ptolemy, Pliny the Elder Vitruvius, and it appears on the Antonine Itinerary. It may also be mentioned in the Book of Ezekiel and the Book of Isaiah

there are special organized tours to the area

Egyptian Oases
Information on the most famous Egyptian oases, including Baharia Oasis, Farafra Oasis, Dakhla Oasis, Kharga Oasis, and Siwa oasis.

Baharia Oasis

Bahariya is most well-known for the so-called Golden Mummies tourist attraction and the Black Desert area. It has many dunes surrounding it as well as hot springs and good hiking routes. Historical antiquities from the Middle Kingdom and two interesting museums are also located in Bawati town. Baharia Oasis is 2,000 square kilometers in size and used to be along an old donkey trading route from Cairo as well as an important center of wine production in ancient Egypt.

Farafra Oasis

Farafra is a small town with a lot of tradition and relaxation. It’s one of the tiniest oases in the Western Desert connecting the area together and is located quite near Libya. It is also situated at the borderline of the start of the White Desert, a beautiful landscape of wind-carved chalk formations. Farafra’s economy is centered on agriculture including growing melons, dates, olives, and rice. Your drive to Farafra Oasis also takes you by Crystal Mountain, which is a very interesting and fun place to visit.

Dakhla Oasis

Dakhla Oasis is located between Farafra and Kharga Oases and is often considered the most picturesque. It has over 500 water sources feeding it from the surrounding area and magenta cliffs, and beautiful verdant gardens. You can get an outstanding view by going to the Badawiya Dakhla Hotel pool and get a good look over the beautiful oasis. Anthropologists believe that thousands of years ago Dakhla had a massive lake where many animals like elephants and bison went to drink.

Kharga oasis

This is also known as the Outer Oasis and is the largest in the Western Desert and the farthest outside Cairo. It lies closest to Luxor and was known in ancient Egypt as the Oasis of Thebes. Kharga is ringed by mountains and sand dunes and has many interesting things to discover including numerous fossils including from dinosaurs.

Siwa oasis

Siwa is the most isolated big oasis in Egypt and is very close to the Libyan border and over 550 km from Cairo. The best way to get there is from Marsa Matruh driving 300 km on the road. Siwa has nice limestone cliffs around it and has the Great Sand Sea to the south as well as various salt lakes that go from being quite big to drying up during the hottest times of the year. There are charming old buildings in Siwa made from mud from the lakes and Siwa is known across Egypt (and the world!) for its delicious dates and olives, not to mention its extraordinary beauty. Siwa is also becoming increasingly known for its drinking water and numerous mineral water companies now produce and ship water from this beautiful oasis.

there are special organized tours to the egyptian oasis

Sharm El Sheikh is an Egyptian city on the southern tip of the Sinai Peninsula, in South Sinai Governorate, on the coastal strip along the Red Sea. Its population is approximately 73,000 as of 2015. Sharm El Sheikh is the administrative hub of Egypt’s South Sinai Governorate, which includes the smaller coastal towns of Dahab and Nuweiba as well as the mountainous interior, St. Catherine and Mount Sinai. The city and holiday resort is a significant centre for tourism in Egypt, while also attracting many international conferences and diplomatic meetings.
Climate
Sharm el-Sheikh
Climate chart (explanation)

The city experiences a subtropical arid climate, classified by the Köppen-Geiger system as hot desert, Temperatures are just short of a tropical climate. Typical temperatures range from 18 to 23 °C (64 to 73 °F) in January and 33 to 37 °C (91 to 99 °F) in August. The temperature of the Red Sea in this region ranges from 21 to 28 °C (70 to 82 °F) over the course of the year

Marsa Alam, Kosseir and Sharm El Sheikh have the warmest winter night temperatures of cities and resorts in Egypt.

The city experiences a subtropical arid climate, classified by the Köppen-Geiger system as hot desert (BWh).[13] Typical temperatures range from 18 to 23 °C (64 to 73 °F) in January and 33 to 37 °C (91 to 99 °F) in August. The temperature of the Red Sea in this region ranges from 21 to 28 °C (70 to 82 °F) over the course of the year.[14] Different sources give different average temperatures for the city.[13][15]

Marsa Alam, Kosseir and Sharm el-Sheikh have the warmest winter night temperatures of cities and resorts in Egypt.

The highest recorded temperature was 46 °C (115 °F) on June 3, 2013, and the lowest recorded temperature was 5 °C (41 °F) on February 23, 2000

Geography and history

Sharm El Sheikh is located on the Egyptian Red Sea coast, at the southern tip of the Sinai Peninsula
Sharm El Sheikh is on a promontory overlooking the Straits of Tiran at the mouth of the Gulf of Aqaba. Its strategic importance led to its transformation from a fishing village into a major port and naval base for the Egyptian Navy. It was occupied by Israel during the Suez Crisis of 1956 and restored to Egypt in 1957. A United Nations peacekeeping force was stationed there until the 1967 Six-Day War when it was recaptured by Israel. Sharm El Sheikh remained under Israeli control until the Sinai peninsula was given to Egypt in 1982 after the Egypt–Israel Peace Treaty of 1979.

A hierarchical planning approach was adopted for the Gulf of Aqaba, whereby their components were evaluated and subdivided into zones, cities and centres. In accordance with this approach, the Gulf of Aqaba zone was subdivided into four cities: Taba, Nuweiba, Dahab and Sharm El Sheikh. Sharm El Sheikh city has been subdivided into five homogeneous centres, namely Nabq, Ras Nusrani, Naama Bay, Umm Sid and Sharm El Maya.

Sharm El Sheikh city, with Naama Bay, Hay el Nour, Hadaba, Rowaysat, Montazah and Shark’s Bay form a metropolitan area.

Before 1967, Sharm El Sheikh was little more than an occasional base of operations for few local fishermen; the nearest permanent settlement was in Nabk, north of Ras El Nasrani (“The Tiran Straits”). Commercial development of the area began when the Israelis built the settlement of Ofira, overlooking Sharm El Maya Bay and the Nesima area, and opened the first tourist-oriented establishments in the area at Naama Bay, 6 kilometres (4 mi) to the north. These included a marina hotel on the southern side of the bay, a nature field school on the northern side, diving clubs, a promenade, and the Naama Bay Hotel.[citation needed] The site off the shore gun emplacements at Ras Nasrani opposite Tiran Island is now a diving area.[4][5][6]

After Sinai was restored to Egypt in 1982, Egypt’s President Hosni Mubarak designated Sharm El Sheikh as The City of Peace and the Egyptian government began a policy of encouraging the development of the city. Foreign and Egyptian investors contributed to building projects including mosques and churches. The city is now an international tourist destination and environmental zoning laws limit the height of buildings to avoid obscuring the natural beauty of the surroundings

there are special organized tours to discover the magic of the area

Marsa Alam is a town in south-eastern Egypt, located on the western shore of the Red Sea. It is currently seeing fast increasing popularity as a tourist destination and development following the opening of Marsa Alam International Airport in 2003.

Among the most famous beaches around Marsa Alam is the Abu Dabab beach. In Abu Dabab, turtles are a common sight. For tourists who seek to see something less typical, there is marine wildlife like crocodile fish and octopuses.

Marsa Alam is also known as a world-class kitesurfing destination and the perfect starting point for safaris
Despite being over 135 miles (217 km) km north of the tropical zone, the city experiences a hot desert climate (Köppen: BWh),[3] with steadier temperatures than places to the north such as Hurghada and Sharm el-sheik, yet Kosseir is steadier and has cooler summers. Marsa Alam, Kosseir, and Sharm el-Sheikh have the warmest night temperatures of all other Egyptian cities and resorts. Average maximum temperatures during January typically range from 22 to 25 °C (72 to 77 °F) and on August 33 to 40 °C (91 to 104 °F).

The temperature of the Red Sea at this location during the year ranges from 22 to 29 °C (72 to 84 °F).[4]

The highest record temperature was 45 °C (113 °F), recorded on May 10, 2010, while the lowest record temperature was 5 °C (41 °F), recorded on January 3, 2008

there are special organized tours to discover the magic of the area

Hurghada was founded in the early 20th century. For many decades it was a small fishing village, but it has grown into a major Red Sea resort as a result of Egyptian and foreign investment that began in the 1980s. Holiday resorts and hotels provide facilities for windsurfing, kitesurfing, yachting, scuba diving, and snorkeling. The city is known for its watersports, nightlife, and warm weather. Daytime temperatures are around 30 °C (86 °F) most of the year, and during July and August temperatures can reach over 40 °C (104 °F). Hurghada is a popular holiday destination for Europeans, especially during the winter, and some spend Christmas and New Year there. Tourist numbers from Russia dropped significantly after the Metrojet Flight 9268 plane crash in November 2015.

Hurghada stretches for about 36 kilometers (22 mi) along the seashore, and it does not reach far into the surrounding desert. The resort is a destination for Egyptian tourists from Cairo, the Delta, and Upper Egypt, as well as package holiday tourists from Europe. Today Hurghada counts 248,000 inhabitants and is divided into:

El Ahia and El Helal, the northern part;
El Dahar (Downtown) is the old part;
Sekalla is the city center;
El Kawsar is the modern part;
El Memsha (Village road) is a pedestrian road stretching over 4 km.
Along with the El, Mamsha can be found many of Hurghada‘s new hotels, restaurants, and shops. Most of the newest and biggest hotel resorts located in the area between Mamsha to Sahl Hasheesh (Village road). After Sahl Hasheesh there is Makadi Bay with its hotels. Dahar is the oldest part of the town, where the town’s traditional bazaar, the post office, and the long-distance bus stations, Go Bus and Upper Egypt Bus are situated. The busiest area is its “city center” Sakala, which is spread along Sheraton Road. There are some hotels, shops, and restaurants along Sheraton Road.[1]

The city is served by the Hurghada International Airport with scheduled passenger traffic connecting to Cairo and directly with several cities in Europe. A new terminal was opened in 2015 to accommodate rising traffic.

Tourism

A fake Lidl store in Hurghada
Although a town in its own right, Hurghada’s current major industry is foreign and domestic tourism, owing to its dramatic landscape, year-round dry and temperate[dubious – discuss] climate, and long stretches of natural beaches. Its waters are clear and calm for most of the year and have become popular for various water-sports, particularly recreational scuba diving and snorkeling.

Dive sites around Abu Ramada Island, Fanadir, Giftun Kebir, and Giftun Soraya are popular. Tourists also visit shipwrecks such as the El Mina or the Rosalie Moller. The beach at Hurghada is not secluded; out to Sigala, the beach is then followed by coastal holiday villages and then desert.

Demographics
Russian residents

Hurghada has 4 schools for Russian children, which are: Galaxy (Созвездие), Our Traditions (Наши Традиции), Dina (Дина) and The World of Knowledge (Мир знаний) (the Russian School Hurghada); as well as the newsletter MK in Egypt. Much of the signage in the city, as of 2015, is in Russian. In June 2015 MK in Egypt publisher Yulia Shevel stated that there were about 20,000 Russians in Hurghada, giving it Egypt’s largest Russian population, though only about 3,000 were officially documented.[10] Russian women staying in Hurghada often marry Egyptian men through an ‘urfi (non-shariah) process.[11]

In 2017 the Russian Consulate was open in Hurghada.[12]

Climate
Hurghada has a subtropical desert climate (Köppen climate classification: BWh), with mild-warm winters and hot to very hot summers. Temperatures in the period December–January–February is warm, but in the evening’s temperature may drop from an average of 20 Celsius degrees to 10. November, March, and April are comfortably warm. May and October are hot and the period from June to September is very hot. The average annual temperature of the sea is 24 °C (75 °F), ranging from 21 °C (70 °F) in February and March to 28 °C (82 °F) in August.

The highest temperature recorded occurred on June 12, 2013, and was 46 °C (115 °F), while the lowest record temperature was recorded on February 2, 1993, and was 0 °C (32 °F).[13]

there are special organized tours to discover the magic of the area

Alexandria, Arabic Al-Iskandariyyah, major city, and urban muḥāfaẓah (governorate) in Egypt. Once among the greatest cities of the Mediterranean world and a center of Hellenic scholarship and science, Alexandria was the capital of Egypt from its founding by Alexander the Great in 332 BCE until its surrender to the Arab forces led by ʿAmr ibn al-ʿĀṣ in 642 CE. One of Egypt’s largest cities, Alexandria is also its principal seaport and a major industrial center. The city lies on the Mediterranean Sea at the western edge of the Nile River delta, about 114 miles (183 km) northwest of Cairo in Lower Egypt. Area city, 116 square miles (300 square km). Population (2006) city, 4,110,015.
Character Of The City
Alexandria has long occupied a special place in the popular imagination by virtue of its association with Alexander and Cleopatra. Alexandria played an important role in preserving and transmitting Hellenic culture to the wider Mediterranean world and was a crucible of scholarship, piety, and ecclesiastical politics in early Christian history. Although it has been asserted that Alexandria declined as a result of its conquest by Muslim Arabs in the 7th century CE, such a statement is misleading. While the city’s political primacy was lost when the capital was moved to the interior, Alexandria remained an important center of naval operations, maritime commerce, and craft production. As late as the 15th century, the city prospered as a transit point in the trade conducted between the Red Sea and the Mediterranean basin.
Landscape
City site
The modern city extends 25 miles (40 km) east to west along a limestone ridge, 1–2 miles (1.6–3.2 km) wide, that separates the salt lake of Maryūṭ, or Mareotis—now partly drained and cultivated—from the Egyptian mainland. An hourglass-shaped promontory formed by the silting up of a mole (the Heptastadion), which was built soon after Alexandria’s founding, links the island of Pharos with the city center on the mainland. It’s two steeply curving bays form the basins for the Eastern Harbour and the Western Harbour.

Climate
The prevailing north wind, blowing across the Mediterranean, gives Alexandria a markedly different climate from that of the desert hinterland. The summers are relatively temperate, although humidity can build up in July and in August, the hottest month when the average temperature reaches 87 °F (31 °C). Winters are cool and invariably marked by a series of violent storms that can bring torrential rain and even hail. The mean daily temperature in January, which is the coldest month, is 64 °F (18 °C).
People
From the late 19th century to the 1980s the population grew 10-fold, the result of high birth rates and migration from the countryside. In the decade following the 1952 revolution, the city’s population reached roughly 1.5 million; by 1976 the population stood at more than 2 million, with half the people under 20 years of age. The city’s population continued to grow, reaching more than 4 million in the early 21st century.

Economy
Manufacturing, finance, and other services
Alexandria’s industrial and commercial activities—manufacturing, shipping, warehousing, banking, food processing, and the production of petrochemicals and cement—indicate the importance of the city’s output for the national economy. Alexandria and its environs account for roughly two-fifths of Egypt’s industrial production. Most industrial development has taken place in the western approaches to the city, around the more modern Western Harbour, and along its southern flank; the industry is the city’s chief employment sector.

The area around the port known as Mīnāʾ al-Baṣal contains warehouses and was once home to the Cotton Exchange. West across the Al-Maḥmūdiyyah Canal is the Al-Qabbārī neighborhood, site of the asphalt works and rice and paper mills. Farther to the west is Al-Maks, with its salt and tanning industries, an oil refinery, a cement works, and, farther on, the limestone quarries. Other industrial development has taken place still farther west in Al-Dukhaylah. To the south lies the area of Al-ʿAmiriyyah, the site of two more refineries, including the Middle East Oil Refinery (Midor), which was designed to meet stringent environmental standards. The lighter industry is concentrated on the banks of the Al-Maḥmūdiyyah Canal.

Agriculture is an important economic activity in the hinterland, and land reclamation has been attempted with some success. In one such project implemented near Alexandria, the Egyptian government has aimed to encourage food production and divert job seekers from overcrowded urban areas by offering graduates of universities and other institutes of higher education parcels of reclaimed land, which they are able to purchase using long-term loans.

Europe’s increasing demand for cotton—introduced into Egypt in the 1820s—was by the 1840s contributing substantially to the city’s wealth. As a result, Alexandria became an increasingly important center for banking and commerce. The Alexandria Stock Exchange, founded in 1883, was followed by the Cairo Stock Exchange in 1903; they eventually linked their operations and continued as the Cairo and Alexandria Stock Exchanges (CASE). Though some banks, such as the Alexandria Commercial and Maritime Bank, are based in Alexandria, a majority of banks—including the Bank of Alexandria—are headquartered in Cairo.

there are special organized tours to discover the magic of alexandria